Cupromakopavonite is a very rare sulfosalt mineral found in hydrothermal deposits. It is typically identified through microscopic examination and chemical analysis due to its visual similarity to other lead-bearing sulfosalts, commonly appearing as metallic gray aggregates.

Hardness
3-4
Mohs
Luster
Metallic
Streak
Gray
Transparency
Opaque

Is this cupromakopavonite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch cupromakopavonite with a known reference. Cupromakopavonite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: gray.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy crystals, granular aggregates.

Often confused with

Cupromakopavonite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside cupromakopavonite

Minerals reported to co-occur with cupromakopavonite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Cu₈Ag₃Pb₄Bi₁₉S₃₈
Mohs hardness
3-4
Density
6.85 g/cm³
Colors
Streak
Gray
Luster
Metallic
Transparency
Opaque
Crystal system
Monoclinic
Crystal habit
Platy crystals, granular aggregates
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
By exsolution from an originally homogeneous high-temperature phase in quartz veins in a metamorphosed hydrothermal scheelite deposit

Where rockhounds find cupromakopavonite

Classic worldwide localities

  • K8 orebody, Felbertal, Salzburg Province, Hohe Tauern, Austria

Field-hunting tip

Where it forms: By exsolution from an originally homogeneous high-temperature phase in quartz veins in a metamorphosed hydrothermal scheelite deposit. If you start seeing makovickyite, over-substituted krupkaite, hodrušite in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify cupromakopavonite?+
Mohs hardness is 3-4. Luster: metallic. The streak is gray. Common colors include gray.
Where is cupromakopavonite found?+
Notable localities include K8 orebody, Felbertal, Salzburg Province, Hohe Tauern, Austria.
Is cupromakopavonite safe to handle?+
Cupromakopavonite contains copper and lead. Contains lead and bismuth; handle with care and wash hands thoroughly after handling. Do not ingest or inhale dust.
What rocks look like cupromakopavonite?+
Cupromakopavonite is most often confused with Galena, Aikinite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with cupromakopavonite?+
Cupromakopavonite commonly co-occurs with Makovickyite, Over-substituted krupkaite, Hodrušite, Kupčikite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does cupromakopavonite form in?+
Where it forms: By exsolution from an originally homogeneous high-temperature phase in quartz veins in a metamorphosed hydrothermal scheelite deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is cupromakopavonite used for?+
Cupromakopavonite is used in collector.

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